Role of inversion tectonics in structural development of the Himalaya

Ashok Kumar Dubey

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Role of inversion tectonics in structural development of the Himalaya

机译：反演构造在喜马拉雅山结构发展中的作用

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Analysis of surface and subsurface structures, variation of shortening amounts obtained by restoration of deformed cross-sections, and occurrence of younger hangingwall rocks over the older footwall rocks across the Vaikrita Thrust in the Higher Himalaya suggests reactivation of early normal faults as thrusts. Based on this, an inversion tectonics model is proposed for structural development of the Himalaya. The model explains the geometrical shape of the Himalaya as primary arcuation and helps in resolving superimposed deformation in the region.

机译：对地表和地下结构的分析，因变形截面的恢复而缩短的量的变化以及喜马拉雅山高地的Vaikrita推力越过较老的下盘壁岩出现的较年轻的上盘壁岩，都表明了早期正常断层作为逆冲的活化。在此基础上，提出了喜马拉雅山构造逆转构造模型。该模型将喜马拉雅山的几何形状解释为主要弧形，并有助于解决该区域中的叠加变形。

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来源
《Journal of Asian earth sciences》 |2010年第6期|p.627-634|共8页
作者
Ashok Kumar Dubey;
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作者单位

Wadia Institute of Himalayan Geology, Dehradun 248 001, India;

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正文语种 eng
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关键词
himalaya; fault reactivation; listric faults; orogeny; thrusting;

机译：喜马拉雅山故障重新激活;李斯特错误造山运动推力;

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Role of inversion tectonics in structural development of the Himalaya

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